
gemstone
Opal (in Jewelry Setting)
Hydrated Silicon Dioxide (SiO2·nH2O)
AI-generated identification · may be incorrectHardness: 5.5-6.5 on Mohs scale. Color: White base with iridescent play-of-color (rainbow flashes). Luster: Subvitreous to waxy. Structure: Amorphous (mineraloid consisting of microscopic silica spheres).
- Hardness
- 5
- Color
- White base with iridescent play-of-color (rainbow flashes)
- Luster
- Subvitreous to waxy
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Physical properties
Hardness: 5.5-6.5 on Mohs scale. Color: White base with iridescent play-of-color (rainbow flashes). Luster: Subvitreous to waxy. Structure: Amorphous (mineraloid consisting of microscopic silica spheres).
Formation & geological history
Formed when silica-rich water precipitates in low-temperature underground cavities and fractures within sedimentary or volcanic rocks. Common in places like Australia and Ethiopia.
Uses & applications
Extensively used in fine and fashion jewelry, such as rings, necklaces, and earrings, as a birthstone (October) and decorative gemstone.
Geological facts
Opals are non-crystalline mineraloids containing up to 20% water trapped within their silica sphere structure. The diffraction of light passing through these tiny spheres creates the gemstone's famous 'play-of-color'.
Field identification & locations
Identified by its characteristic flashes of spectral color (play-of-color) against a white, clear, or dark background. Usually cut into cabochons or small inlaid stones in band rings.
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